Carbon, soot and particles from combustion end up in deep-sea trenches
New research shows that disproportionately large amounts of carbon accumulate at the bottom of deep-sea trenches. The trenches may thus play an important role for deep-sea storage of organic material - and thus for the atmospheric Co2 balance.
The Earth's deep-sea trenches are some of the least explored places on Earth - as they are very difficult to access, are pitch black and the pressure is extremely high. Collecting samples and making reliable measurements of the processes that regulate the turnover of organic material in the deep is therefore difficult.
In recent years, however, researchers from the Danish Center for Hadal Research (HADAL) at University of Southern Denmark have carried out a number of expeditions to deep-sea trenches.
They have developed and applied sophisticated underwater robots, and they have demonstrated in several published studies that the steep deep-sea trenches accumulate various material including organic carbon that ends up at the bottom of the trenches.
The bottom of a deep-sea trench can therefore be a veritable deposition hotspot for microbial life forms that converts the material.
Carbon accumulates in the trenches
In three recent studies, the researchers report that hard-to-decompose organic carbon, including so-called black carbon, accumulates in large quantities at the bottom of the trenches. The studies can be found here, here and here.
Black carbon consists of particles formed during burning of fossil fuels, wood and forests; activities that also lead to the release of CO2. The occurrence of black carbon is thus an indicator of the extent of fossil burning. The particles themselves can also contribute to warming, as they are carried by wind and weather to ice-covered areas, e.g. polar regions, where they settle on ice and snow, increasing heat absorption and thus the melting.
- And now we see that large amounts of black carbon end up at the bottom of deep-sea trenches, says Ronnie N. Glud, professor and head of the Danish Center for Hadal Research.
Samples from more than six kilometers depth
More concretely, the research team has calculated that every year, somewhere between 500,000 and 1,500,000 tonnes of black carbon is stored in the hadal deep-sea; that is the part of the seabed that lies at a depth of more than six kilometers.
In comparison, 6,600,000 – 7,200,000 tonnes of black carbon are emitted annually from the burning of fossil fuels.
The researchers base their calculations on sediment samples that they have retrieved from various deep-sea trenches, exceeding six km deep and thus part of the hadal realm. The hadal zone covers 1% of the seabed.
Not only are disproportionately large amounts of black carbon being deposited in the deep; the same happens for other resilient, hard-to-decompose carbons. In fact, the studies show that every square meter in the central parts of a deep-sea trench buries 70 times more resilient carbon compared to the deep sea in general.
Meet the researcher
Ronnie N. Glud is a professor at the Department of Biology, Chair at the Danish Institute for Advanced Study (DIAS) and head of the Danish Center for Hadal Research. As a deep-sea researcher, he has led and participated in many expeditions to deep-sea trenches. This interview was conducted just after his return from The Aleutian Trench off Alaska and before he went on to the South Sandwich Trench near the Falkland Islands. The research is supported by Danish National Research Foundation, the European Research Council and the Independent Research Fund Denmark.